There is no abstract created for this record

In order to test the recently acquired resistivity equipment a series of test points were located in the University grounds. From the results of this survey, a cross section was drawn which was found to correspond with subsurface conditions...

The results of this investigation show a small gravity "low" over the structure suggesting that the rock formations beneath the central portion of the Dome are less dense than those comprising the surrounding area. No significant magnetic variations...

Following aerial ground geophysics reconnaissance drilling of 2 zones had intersected iron formation over 5.5 miles EW, 600'-1000' Ns and to depths of 850'. The formaiton appears to average 25% iron oxide, is relativley course grained and Davis Tube...

There is no abstract created for this record

There is no abstract created for this record

There is no abstract created for this record

The testing of iron ores for beneficiation by magnetic separation is normally done in laboratory separators of various types and the results are reported in terms of the variables, such as magnet coil current, rotor speed and gap width, of the...

In March 1964 a resistivity survey was performed in the Polda Basin to determine the depths to the water table in an area of three square miles approximately 26 miles west of Lock. Although the field methods used produced unreliable results, it is...

The author spent eleven months in the United States of America (September 1963 to July 1964) as an exchange visitor. He was engaged as party leader on a deep resistivity study of the earth's crust in Orogon and Washington States. The work was later...

Ten ground magnetic and gravity traverses delineated the Carrow Anomaly. Seven drillholes disclosed iron formation up to 200 ft. wide. Assuming a stike length of 3000 ft., reserves could approach 6 million tonnes per 100 ft. assaying 23.0 - 28.6%...

A ground magnetic survey was carried out over an aeromagnetic anomaly to measure the vertical component of the earth's field. The results are presented as profiles and contours and a site proposed for a diamond drill hole on the basis of the...

The purpose of this refraction seismic and resistivity survey was to determine the nature of the bedrock in the area of the proposed freeway near Crafers. The results indicate that the sandstone bedrock is strongly weathered to depths of at least...

Originally confined to the Cornish Copper line, the geophysical investigation was extended to cover the Tarcoola Blocks, Afghan Camp and also Brown Hill areas of workings. Resistivity contours supply some information as to the structure in the areas...

Drilling results confirm the general synclinal structure. The jaspilite complex appears to be too low grade, too deeply weathered and too narrow to be of immediate economic interest. The western flank and main synclinal axis need more exploration for...

In November 1964 this exploratory survey found good hydrological - geophysical correlation for the sedimentary formations to depths of 100 feet in the Murray River irrigation areas between Waikerie and Renmark. Analysis indicates that the sands,...

There is no abstract created for this record

There is no abstract created for this record

There is no abstract created for this record

The history of the project, tabulated geophysical results, summarised bore logs (KR's 1-11) with the grade of the iron formations intersected are recorded. Recommendations are made for further ground geophysics and drilling.